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Chicago · October 11, 2026

Heat and marathon pace

A warmer race puts new demands on the body. The physiology, research and interactive pace model show why conditions matter, and what a model can tell us.

One circulation, two demands

Working muscles need oxygen. As the body heats up, more blood also flows to the skin to release heat. Sustaining movement and cooling the body both depend on the circulation.

Heart and circulation

Blood supplies both working muscles and skin.

Working muscles

Oxygen for movement

Blood carries the oxygen needed to sustain the effort of running.

Skin

Blood flow for cooling

More blood carries heat toward the skin. Sweat removes heat as it evaporates.

The same pace can require more effort in the heat.

Cooling adds to the demands of exercise. This diagram explains the mechanism; it does not show measured blood-flow shares or a personal time penalty.

Built with AI · Jenn Umanzorjennumanzor.com · Chicago heat guide
Simmons et al., 2011 · physiology review

Temperature and pace

An ideal-conditions goal sets the baseline. Changing the air temperature reveals the site’s illustrative pace adjustment, with other conditions held fixed.

Ideal-conditions goal
6:55/miEstimated pace
3:01:09Estimated finish
+1.2%Modeled time
Air temperature and estimated marathon pace6:456:577:097:227:34Pace (min/mile) · slower ↑40°F50°F60°F70°F80°F

Green line: illustrative pace. Blue marker: selected temperature. Dew point is fixed at 40°F; wind and sun penalties are excluded. This is a planning heuristic, not a measured personal response or a safe-racing threshold.

Exact values and calculation
AirPace / mileFinish
40°F6:502:59:00
50°F6:502:59:00
55°F6:523:00:04
60°F6:553:01:09
65°F7:013:03:50
70°F7:073:06:31
75°F7:183:11:26
80°F7:293:16:22

The model adds 0.12 percentage points per °F above 50 through 60, then 0.30 through 70, then 0.55 above 70. Finish time is the baseline multiplied by that factor. These coefficients are assumptions, not a regression reproduced from the research.

More than a thermometer

Air temperature is only one part of the exposure. Conditions also change over the hours spent on the course.

Humidity

Sweat cools as it evaporates. Humid air limits that evaporation.

Sun

Radiant heat adds to the load, even at the same air temperature.

Wind

Air movement changes heat exchange. The thermometer alone cannot describe it.

04 · Reading the evidence

What the research can tell us

Marathon performance

Warmer conditions, slower performances

Ely and colleagues studied marathon results across wet-bulb globe temperature categories and found progressively slower performances in warmer categories.

WBGT accounts for environmental heat stress. It is not interchangeable with the air-temperature slider above.

Ely et al., 2007 · read the abstract
Physiology

Cooling has a circulatory cost

Simmons and colleagues review how increased skin blood flow supports heat loss and adds to cardiovascular demands during exercise in the heat.

The mechanism helps explain the challenge. It does not assign a fixed share of blood to the skin or establish one runner’s exact slowdown.

Simmons et al., 2011 · read the review
Research → planning model

The research supports the direction of the effect. The calculator’s coefficients are explicit planning assumptions. Neither study establishes Jenn’s exact Chicago time penalty.